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RECORD NUMBER: 18 OF 48

Main Title Paleoecological Investigation of Recent Lake Acidification in the Adirondack Mountains, N. Y.
Author Charles, D. F.; Binford, M. W.; Furlong, E. T.; Hites, R. A.; Mitchell, M. J.;
CORP Author Indiana Univ. at Bloomington. ;State Univ. of New York at Albany. Coll. of Environmental Science and Forestry. ;Harvard Univ., Cambridge, MA. Graduate School of Design.;Corvallis Environmental Research Lab., OR.;National Science Foundation, Washington, DC.
Publisher c1990
Year Published 1990
Report Number EPA/600/J-90/266;
Stock Number PB91-144709
Subjects Acid rain; Paleoecology; Lakes; Sediments; pH; Water chemistry; Graphs(Charts); Environmental monitoring; Adirondack Mountains; Reprints;
Holdings
Library   Call Number Additional Info Location Date Modified
NTIS PB91-144709 Most EPA libraries have a fiche copy filed under the call number shown. Check with individual libraries about paper copy. NTIS 06/13/1991
Collation 49p
Abstract Paleoecological analysis of the sediment record of 12 Adirondack lakes reveals that the 8 clearwater lakes with current pH<5.5 and alkalinity <10 microeq/l have acidified recently. The onset of the acidification occurred between 1920 and 1970. Loss of alkalinity, based on quantitative analysis of diatom assemblages, ranged from 2 to 35 microeq/l. The acidification trends are substantiated by several lines of evidence including stratigraphies of diatom, chrysophyte, chironomid, and cladoceran remains, Ca:Ti and Mn:Ti ratios, sequentially extracted forms of Al, and historical fish data. Acidification trends appear to be continuing in some lakes, despite reductions in atmospheric sulfur loading that began in the early 1970s. The primary cause of the acidification trend is clearly increased atmospheric deposition of strong acids derived from the combustion of fossil fuels. Natural processes and watershed disturbances cannot account for the changes in water chemistry that have occurred, but they may play a role. Sediment core profiles of Pb, Cu, V, Zn, S, polycyclic aromatic hydrocarbons, magnetic particles, and coal and oil soot provide a clear record of increased atmospheric input of materials associated with the combustion of fossil fuels beginning in the late 1800s and early 1900s.
Supplementary Notes Pub. in Jnl. of Paleolimnology 3, p195-241 1990. Prepared in cooperation with State Univ. of New York at Albany. Coll. of Environmental Science and Forestry, and Harvard Univ., Cambridge, MA. Graduate School of Design. Sponsored by Corvallis Environmental Research Lab., OR., and National Science Foundation, Washington, DC.
NTIS Title Notes Journal article.
Title Annotations Reprint: Paleoecological Investigation of Recent Lake Acidification in the Adirondack Mountains, N. Y.
Category Codes 68A
NTIS Prices PC A03/MF A01
Primary Description 600/02
Document Type NT
Control Number 109129700
Cataloging Source NTIS/MT
Origin NTIS
Type CAT